ware left and, are found* 
The successful form, completed or tested 
as to the workable qualities of the material, mere carried away to 
be applied to their appropriate uses or to jo fi is'n . at leisure. 
This resulted in general in a separation of the two classes of 
chipped stones| the rude rejected forms resulting from irqperfeet 
•flecture and very generally from too great thickness, a thin blade 
being the principal form do sliced, were left on the shaping sites 
and these with the passing of time were often deeply buried[ through 
changes in the loosely bedded deposits* while the accepted form 
were reroved to the village sites to be .finished and used* Here 
we have the root of the first 
As a re 
f \ *. • >l 3Hp f 
suit of the conditions described, our early and inexperienced col- 
W ft t ?> fay <J A***i^*4tA' 
lectors, not appreciating the real conditions ti^.-^ndicated, reached 
*M & if 1*4 jdl \A ** 
the conclusion that the rude rejected forms belonged as original 
inclusions in, or had been weathered out of, the exposed margins 
% deposits where they hafete^i 
of the 
found. The observation that these rudely chipped forms correspond 
in simplicity and general type of form with the ”stone Implements w 
